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Precautionary spatial protection to facilitate the scientific study of habitats and communities under ice shelves in the context of recent, rapid, regional climate change

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TLDR
In this article, the authors highlight why commercial fishing activities should not be permitted in these habitats, and suggest that areas under existing ice shelves in Subareas 88.3, 48.1 and 48.5 should be preserved and protected for scientific study.
Abstract
Recent rapid climate change is now well documented in the Antarctic, particularly in the Antarctic Peninsula region. One of the most evident signs of climate change has been ice-shelf collapse; overall, 87% of the Peninsula’s glaciers have retreated in recent decades. Further ice-shelf collapse will lead to the loss of existing marine habitats and to the creation of new habitats, with consequent changes in both ecological processes and in community structure. Habitats revealed by collapsed ice shelves therefore offer unique scientific opportunities. Given the complexity of the possible interactions, and the need to study these in the absence of any other human-induced perturbation, this paper highlights why commercial fishing activities should not be permitted in these habitats, and suggests that areas under existing ice shelves in Subareas 88.3, 48.1 and 48.5 should be preserved and protected for scientific study. The boundaries of these areas should henceforth remain fixed, even if the ice shelves recede or collapse in the future. Designation of areas under ice shelves as areas for scientific study would fulfil one of the recommendations made by the Antarctic Treaty Meeting of Experts in 2010.

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Linkages between vulnerability, resilience, and adaptive capacity

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Consensus management in Antarctica's high seas – past success and current challenges

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Southern Ocean fishery management - Is CCAMLR addressing the challenges posed by a changing climate?

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References
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Journal ArticleDOI

Ice-Shelf Melting Around Antarctica

TL;DR: Detailed glaciological estimates of ice-shelf melting around the entire continent of Antarctica show that basal melting accounts for as much mass loss as does calving, making ice- shelf melting the largest ablation process in Antarctica.
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Ice sheet grounding line dynamics: Steady states, stability, and hysteresis

TL;DR: In this paper, the results of boundary layer theory for ice flux in the transition zone against numerical solutions that are able to resolve the transition zones were verified. But the results were not applied to the large-scale dynamics of a marine ice sheet.
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Retreating glacier fronts on the Antarctic Peninsula over the past half-century.

TL;DR: The continued retreat of ice shelves on the Antarctic Peninsula has been widely attributed to recent atmospheric warming, but there has been little published work describing changes in glacier margin positions as discussed by the authors, which suggests that this may not be the sole driver of glacier retreat in this region.
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Warming of the Southern Ocean since the 1950s.

TL;DR: Autonomous Lagrangian Circulation Explorer floats recorded temperatures in depths between 700 and 1100 meters in the Southern Ocean throughout the 1990s, suggesting that mid-depth Southern Ocean temperatures have risen 0.17°C between the 1950s and the 1980s.
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